Khodzhakul Formation | |
Type: | Geological formation |
Age: | Cenomanian ~ |
Period: | Cenomanian |
Prilithology: | Sandstone |
Region: | Karakalpakstan |
Coordinates: | 40.1°N 65.8°W |
Paleocoordinates: | -35.9°N 65.5°W |
Underlies: | Tamdytruba & Bissekty Formations |
Overlies: | Bortesken Formation |
The Khodzhakul Formation is a Cenomanian aged geologic formation in Uzbekistan. Dinosaur remains are among the fossils that have been recovered from the formation.[1] As well as those of Mammals.[2] It is part of the same stratigraphic succession as the overlying Bissekty Formation.
One of the largest mammals of the Mesozoic, Oxlestes, occurred in this formation, and may have predated on dinosaur species.[3]
Dinosaurs | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Asiaceratops[4] | A. salsopaludalis |
| "Teeth, cranial fragments, phalanx."[5] | |||
Gilmoreosaurus[6] | G. atavus |
| ||||
Horezmavis[7] | H. eocretaceous |
| "Tarsometatarsus."[8] | |||
Kulceratops | K. kulensis |
| "Fragmentary material." | |||
Therizinosauroidea | Indeterminate[9] | Upper | ||||
Pectinodon | P. Sp |
| ||||
Mammals | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images | |
Bobolestes | B. zenge | Maxilla and dentary fragments | Zalambdalestoidea | ||||
Eozhelestes | E. mangit | dentary fragments and teeth | |||||
Sheikhdzheilia | S. rezvyii | Maxilla and dentary fragments | ?Zhelestidae | ||||
Zalambdalestidae | Indeterminate | Right petrosal | |||||
‘‘Zhelestidae’’ | Indeterminate | Left dentary and dentary fragment | Large taxon |